Rock Identifier
Granodiorite (Gneissic texture) (Granodiorite (containing Quartz SiO2, Plagioclase Feldspar, and Biotite)) — igneous
igneous

Granodiorite (Gneissic texture)

Granodiorite (containing Quartz SiO2, Plagioclase Feldspar, and Biotite)

Hardness: 6-7 (Mohs scale); Color: Salt and pepper (gray, white, black); Luster: Dull to vitreous; Crystal structure: Phaneritic/Medium-grained; Cleavage: Poor; Specific gravity: 2.6-2.7

Hardness
6-7 (Mohs scale)
Color
Salt and pepper (gray, white, black)
Luster
Dull to vitreous
Identified More igneous

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Physical properties

Hardness: 6-7 (Mohs scale); Color: Salt and pepper (gray, white, black); Luster: Dull to vitreous; Crystal structure: Phaneritic/Medium-grained; Cleavage: Poor; Specific gravity: 2.6-2.7

Formation & geological history

Formed from the slow cooling of silica-rich magma below the Earth's surface. This specimen appears to have mild metamorphic alignment (gneissic character), suggesting it was subjected to heat and pressure after its initial igneous formation.

Uses & applications

Used primarily in heavy construction, road base, and as decorative dimension stone (frequently sold as 'granite' in the countertop industry).

Geological facts

Granodiorite is the rock that makes up the famous Rosetta Stone. It is the intermediate rock between granite and diorite, containing more plagioclase than orthoclase feldspar.

Field identification & locations

Identify by its 'salt and pepper' appearance and hardness (it will scratch glass). Look for the presence of translucent quartz crystals nestled between opaque white feldspars and black mica flakes. Commonly found in large batholiths like the Sierra Nevada mountains.